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The ScanMars radar onboard AMADEE-18 analog mission to Mars Alessandro Frigeri (1), Maurizio Ercoli (2), Cristina Pauselli (2), Gernot Groemer (3) (1) Istituto di Astrofisica e Planetologia Spaziali, INAF, Rome, Italy ([email protected], Phone:+39-06-4993-4227); (2) Università degli Studi di Perugia, Perugia, Italy; (3) Österreichisches Weltraum Forum, Austrian Space Forum, Innsbruck, Austria. Abstract Simulated, or analog, planetary missions are putting the base for the forthcoming extraterrestrial explorations, testing new technologies and refining existing operative exploration procedures [1, 2, 3]. In February 2018, the Austrian Space Forum led an international Mars analog mission in the Dhofar region, Oman. Directed by a Mission Support Center in Aus- tria, a small field crew conducted experiments preparing for future human Mars missions in the fields of engi- neering, planetary surface operations, astrobiology, geo- physics/geology and life sciences. In summer 2017 our ScanMars experiment has been selected to be part of the mission. ScanMars employed a Ground Penetrating Radar to investigate the subsurface by transmitting and receiving radio-wave impulses into the ground. The expected results of the experiment are geophysical images of the underground structures, mate- rial differences and the presence of groundwater[4]. Here we present the ScanMars experiment and its re- sults from AMADEE-18 analog mission to Mars, in the Oman desert. 1 Introduction The instrumental part of the ScanMars experiment onbo- rard AMADEE-18 consists of a Zond-12e Ground Pene- trating Radar, developed by Radsys, Latvia. We choose the 500 MHz operative frequency as a good compromise between resolution, penetration depth and maneuverabil- ity. The experiment can be divided in three phases: the training, the scientific campaign and the scientific syn- thesis. Figure 1: Analog astronauts testing operative procedures during the training at OEWF headquarters in Innsbruck, Austria. 2. Training Phase The most different element from ScanMars a common radar fieldwork is undoubtedly the fact that the data was going to be acquired by the analog astronauts and not the scientists. Thus the astronauts’ training becomes a crit- ical part of the experiment. The challenge of this phase resides in the fact that the analog astronauts have a back- ground which is not specifically trimmed on the exper- iment, and that they have to acquire a large quantity of diverse information during the training (Figure 1). 3. Scientific campaign The training efforts have been put into practice during the ScanMars scientific campaign in the field in the Dhofar (Figure 2), where the field crew operated the radar over the planned scientific targets. The experiment explored four different sites with slight different geologic charac- EPSC Abstracts Vol. 12, EPSC2018-300-1, 2018 European Planetary Science Congress 2018 c Author(s) 2018 E P S C European Planetary Science Congress
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Page 1: Abstract - Copernicus.org...international Mars analog mission in the Dhofar region, Oman. Directed by a Mission Support Center in Aus-tria, a small eld crew conducted experiments preparing

The ScanMars radar onboard AMADEE-18 analog mission to Mars

Alessandro Frigeri (1), Maurizio Ercoli (2), Cristina Pauselli (2), Gernot Groemer (3)(1) Istituto di Astrofisica e Planetologia Spaziali, INAF, Rome, Italy ([email protected], Phone:+39-06-4993-4227); (2)Università degli Studi di Perugia, Perugia, Italy; (3) Österreichisches Weltraum Forum, Austrian Space Forum, Innsbruck, Austria.

Abstract

Simulated, or analog, planetary missions are putting thebase for the forthcoming extraterrestrial explorations,testing new technologies and refining existing operativeexploration procedures [1, 2, 3].

In February 2018, the Austrian Space Forum led aninternational Mars analog mission in the Dhofar region,Oman. Directed by a Mission Support Center in Aus-tria, a small field crew conducted experiments preparingfor future human Mars missions in the fields of engi-neering, planetary surface operations, astrobiology, geo-physics/geology and life sciences.

In summer 2017 our ScanMars experiment has beenselected to be part of the mission. ScanMars employeda Ground Penetrating Radar to investigate the subsurfaceby transmitting and receiving radio-wave impulses intothe ground. The expected results of the experiment aregeophysical images of the underground structures, mate-rial differences and the presence of groundwater[4].

Here we present the ScanMars experiment and its re-sults from AMADEE-18 analog mission to Mars, in theOman desert.

1 Introduction

The instrumental part of the ScanMars experiment onbo-rard AMADEE-18 consists of a Zond-12e Ground Pene-trating Radar, developed by Radsys, Latvia. We choosethe 500 MHz operative frequency as a good compromisebetween resolution, penetration depth and maneuverabil-ity. The experiment can be divided in three phases: thetraining, the scientific campaign and the scientific syn-thesis.

Figure 1: Analog astronauts testing operative proceduresduring the training at OEWF headquarters in Innsbruck,Austria.

2. Training PhaseThe most different element from ScanMars a commonradar fieldwork is undoubtedly the fact that the data wasgoing to be acquired by the analog astronauts and not thescientists. Thus the astronauts’ training becomes a crit-ical part of the experiment. The challenge of this phaseresides in the fact that the analog astronauts have a back-ground which is not specifically trimmed on the exper-iment, and that they have to acquire a large quantity ofdiverse information during the training (Figure 1).

3. Scientific campaignThe training efforts have been put into practice during theScanMars scientific campaign in the field in the Dhofar(Figure 2), where the field crew operated the radar overthe planned scientific targets. The experiment exploredfour different sites with slight different geologic charac-

EPSC AbstractsVol. 12, EPSC2018-300-1, 2018European Planetary Science Congress 2018c© Author(s) 2018

EPSCEuropean Planetary Science Congress

Page 2: Abstract - Copernicus.org...international Mars analog mission in the Dhofar region, Oman. Directed by a Mission Support Center in Aus-tria, a small eld crew conducted experiments preparing

Figure 2: The analog astronauts during ScanMars exper-iment data acquisition. The radar sledge is being pulledalong the planned profile.

Figure 3: A data frame extracted from the experiment re-sults. The radargram is the visual representation of theradar echoes recorded in the field, representing distancealong the profile (horizontal) versus time delay (vertical).

teristics. The analog astronauts acquired about 1400 me-ters of profiles. A total of about 70000 radar echoes havebeen recorded and returned to the scientific data archive.

4. ResultsFigure 3 shows one of the 25 radargrams which have beenacquired in the field. The data quality is very good andthe radar echoes show extremely well geologic featurestypical of the wadi riverbed. The penetration depth of thesignals is about 5 meters, and in some case we can extractdeeper information.

5. ConclusionsThe ScanMars experiment can be considered successfulnot just because of the data acquired but more importantlywe consider ScanMars a success due to the volume of newexperience created among the scientific team, the oper-ations’ team and the field crew. A good teamwork hasbeen necessary to face the problems which are difficult,when not impossible, to foresee beforehand. With Scan-Mars and AMADEE-18 in general we are understandingthe different aspects of scientific exploration of distantworlds, developing strategies and workflows which willbe the building blocks of the future human planetary mis-sions.

AcknowledgementsThanks to the AMADEE-18 personnel, from the astro-nauts, the field crew and the mission control, whose ef-forts turned the ScanMars experiment into a success. Weare grateful to the volunteers of the Italian Radio Ama-teur Association (ARI) who assisted us in laboratory mea-surements and system optimization of the ScanMars radarhardware.

References[1] Snook and Mendell, The need for analogue missions in sci-

entific human and robotic planetary exploration. 35th LPSC,abstract #2130, 2004

[2] Groemer, G. et al., 47th LPSC, abstract #1903, 2016

[3] Rossi, A. P. et al., Augmented field Geology and Geo-physics for Planetary Analogues, Eropean GeophysicalUnion, Vienna, 2018

[4] Annan, A. and Davis, J. L., Ground penetrating radar forhigh-resolution mapping of soil and rock stratigraphy. Geo-physical Prospecting 37, 531-551, 2018


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